Convectional rain occurs when the sun heats the Earth's surface, causing the air above it to become warm and rise. As the warm air rises, it cools and condenses, forming clouds. When the condensation reaches a point where the water droplets in the clouds become too heavy, they fall to the ground as rain. This process is known as convectional rain.
Convectional rain is caused by the heating of the Earth's surface by the sun, which in turn causes the air above it to become warm and rise.
As the warm air rises, it cools and condenses, forming clouds. These clouds eventually lead to the formation of rain.
Condensation occurs as the warm air rises and cools, leading to the formation of water droplets in the clouds. These water droplets eventually become heavy enough to fall as rain.
Convectional rain is most commonly observed in tropical regions, where the sun's heat is intense and the air near the surface becomes very warm, leading to strong convection currents.
Understanding convectional rain is important for comprehending the water cycle and the factors that contribute to precipitation in different regions of the world.
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